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气候变化和地下水开采对中国滦河流域玉米中重金属含量时空变化的影响。

The effects of climate change and groundwater exploitation on the spatial and temporal variations of heavy metal content in maize in the Luan River catchment of China.

机构信息

Institute of Hydrogeology and Environmental Geology, Shijiazhuang, 050061, China.

出版信息

Environ Sci Pollut Res Int. 2020 Jan;27(1):1035-1052. doi: 10.1007/s11356-019-07012-x. Epub 2019 Dec 9.

Abstract

The effects of climate change and anthropogenic activities on the concentration of heavy metal in maize were quantitatively characterized in this study to help us better understand the complex interactions among the groundwater, vadose, plant, and atmosphere layers in the critical zone. We hypothesized that climate change and groundwater resource exploitation firstly affected the shallow groundwater level, and then the groundwater table fluctuation (GTF) impacted the concentration of heavy metal in maize through the critical zone (CZ) structure and parameters. To test our hypothesis, we collected 960 soil and 288 maize samples from the Luan River catchment in the North China Plain. The Groundwater Modeling System software was used to describe the effects of precipitation and groundwater resource exploitation on the groundwater table, and then, the structural equation method was employed to characterize the quantitative effects of GTF, precipitation, and air temperature on the concentration of heavy metal in maize. The results indicate that the influence coefficients of the effects of climate change and anthropogenic activities on the concentrations of Fe, Mn, Cr As, Pb, and Sr were 0.1595, 0.088, 0.0042, - 0.0092, 0.2219, and 0.0493 in the north plain, respectively, and 0.0256, 0.0151, 0.0816, - 0.2264, 0.1125, and - 0.0106 in the south plain of the study region, respectively. Since the human health risks of metals were mainly attributed to Fe, Mn, and Cr in the Luan River catchment, increasing the groundwater resource exploitation volume is an effective way to decrease the Fe, Mn, and Cr contents in maize by decreasing the shallow groundwater table.

摘要

本研究定量刻画了气候变化和人为活动对玉米中重金属浓度的影响,有助于更好地理解地下水-包气带-植被-大气连续体(CZ)中各圈层间的复杂相互作用。我们假设气候变化和地下水资源开采首先影响浅层地下水位,然后通过 CZ 结构和参数,地下水位波动(GTF)影响玉米中重金属的浓度。为了验证我们的假设,我们在华北平原的滦河流域采集了 960 个土壤样本和 288 个玉米样本。地下水模拟系统软件被用来描述降水和地下水资源开采对地下水位的影响,然后,结构方程方法被用来刻画 GTF、降水和气温对玉米中重金属浓度的定量影响。结果表明,在研究区的北平原,气候变化和人为活动对 Fe、Mn、Cr、As、Pb 和 Sr 浓度的影响系数分别为 0.1595、0.088、0.0042、-0.0092、0.2219 和 0.0493,而在南平原的影响系数分别为 0.0256、0.0151、0.0816、-0.2264、0.1125 和-0.0106。由于在滦河流域金属对人体健康的危害主要归因于 Fe、Mn 和 Cr,因此增加地下水资源开采量是通过降低浅层地下水位降低玉米中 Fe、Mn 和 Cr 含量的有效途径。

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